摘要
湖南片状高岭土矿床丰富多采,按成因可分为两大类五个亚类。不同类型矿床的控矿因素不尽相同。风化残余型片状高岭土矿床主要受母岩、风化程度、地形、地貌等因素的控制。沉积型片状高岭土矿床主要受古地理环境的控制。
The Schistose Kaolinite deposits in Hunan are rich and varing in types, Which can be genetically classified into two types and 5 Subtypes. The metallogenic factors are different for different type of deposit. The weathering-residue type is mainly controlled by hostrock, weathering degree, landform and landscape etc; The sedimen tary type is mainly controlled by the paleogeographic enviroments.
出处
《湖南地质》
1989年第1期44-50,共7页
Hunan Geology
关键词
高岭土矿床
成因类型
挖矿因素
kaolinite deposit
Genetic type
Metallogenic factors
Hunan
